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南半球白垩纪-古近纪之交生物灭绝期孢粉地层学
作者姓名:Vivi VAJDA  Antoine BERCOVICI
作者单位:瑞典隆德大学地质学系;生物地质与环境地质国家重点实验室,中国地质大学(武汉)
基金项目:国家自然科学基金(No.91114201);国家重点基础研究发展计划(2012CB821906)资助出版;support from the Royal Swedish Academy of Sciences through the Knut and Alice Wallenberg Foundation;the Swedish Research Council(Grant No.2007-4509);the Lund University Pufendorf Institute Astrobiology funding
摘    要:白垩纪-古近纪(K-Pg)生物大灭绝事件前后的孢粉植物群的变化,可以详细揭示植被对一场全球环境危机(6550万年前小行星撞击现今的墨西哥)的响应。在K-Pg界线处有一些植物门类灭绝了,因此孢粉地层学是确定非海相序列中白垩纪-古近纪界线的主要工具。南半球包括以下植物区:热带至亚热带棕榈植物大区,高纬度Nothofagidites/Proteacidites大区,以及一个含有混合的植物组分的过渡区域。在棕榈植物大区,一些马斯特里赫特期的关键物种在白垩纪-古近纪界线处灭绝了,包括Aquilapollenites magnus、Buttinia andreevi、Crassitricolporites brasiliensis、Proteaci ditesdehaani和Gabonisporis vigourouxii。在Nothofagidites/Proteacidites大区,Tricolporite slilliei、Triporopollenites sectilis、Quadraplanus brossus、Nothofagidites kaitangata和Grapnelispora evansii等物种最后出现于白垩纪-古近纪界线处。由此可见,我们需要对南半球与中国的K-Pg界线处的孢粉信息进行更详尽的分析,才能更详细地了解不同纬度、不同地点的植被对墨西哥尤卡坦撞击事件的响应。

关 键 词:生物地层学  孢粉学  孢子  花粉  集群灭绝  白垩纪  古近纪南半球

POLLEN AND SPORE STRATIGRAPHY OF THE CRETACEOUS-PALEOGENE MASS-EXTINCTION INTERVAL IN THE SOUTHERN HEMISPHERE
Vivi VAJDA,Antoine BERCOVICI.POLLEN AND SPORE STRATIGRAPHY OF THE CRETACEOUS-PALEOGENE MASS-EXTINCTION INTERVAL IN THE SOUTHERN HEMISPHERE[J].Journal of Stratigraphy,2012(2):153-164.
Authors:Vivi VAJDA  and Antoine BERCOVICI
Institution:1) Department of Geology,Lund University,Lund S lvegatan 12,22362,Sweden,2) State Key Laboratory of Biogeology and Environmental Geology,China University of Geosciences,Wuhan 430074,China
Abstract:The palynofloral changes around the Cretaceous-Paleogene(K-Pg) mass extinction event reveal the fine details of vegetation response to a global environmental crisis-in this case an asteroid impact in Mexico 65.5 million years ago.Due to the extinction of several plant taxa at the K-Pg boundary,palynostratigraphy is a prime tool for localizing the Cretaceous-Paleogene boundary in non-marine successions.The Southern Hemisphere includes the tropical to sub-tropical Palmae Province,the high-latitude Nothofagidites/Proteacidites Province,and a transitional zone of mixed floristic composition.Maastrichtian key-species that go extinct at the Cretaceous-Paleogene boundary within the Palmae Province include Aquilapollenites magnus,Buttinia andreevi,Crassitricolporites brasiliensis,Proteacidites dehaani and Gabonisporis vigourouxii.In the Nothofagidites/Proteacidites Province,taxa such as Tricolporites lilliei,Triporopollenites sectilis,Quadraplanus brossus,Nothofagidites kaitangata,and Grapnelispora evansii have their last appearances at the boundary.It is obvious that more thorough analyses of the palynological signals across the K-Pg boundary in theSouthern Hemisphere and China are required to elucidate the detailed patterns of vegetation response at different latitudes and at varying distances from the impact site in Yucatan,Mexico.
Keywords:biostratigraphy  palynology  pollen  spores  mass-extinction  Cretaceous  Paleogene  Hemisphere
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